Comparatively little is known about the pre-bog soils <strong>of</strong> <strong>North</strong> <strong>Mayo</strong>. A crude distinction may have existed between soils developed over Carboniferous lime- <strong>and</strong> s<strong>and</strong>stones <strong>and</strong> those on the Dalradian <strong>and</strong> older rock to the west, with the Carboniferous areas likely to have had higher quality soils with better drainage <strong>and</strong> productivity. However, this will have been moderated by the tills, glacio-marine <strong>and</strong> marine muds <strong>and</strong> other superficial deposits consequent upon deglaciation. Variation at a small scale is likely to have been significant, <strong>and</strong> exposure to winds important in determining farming potential. 104
References ?? Soil Map <strong>of</strong> West <strong>Mayo</strong>. Brooks, A., <strong>and</strong> R. Edwards. 2006. The Development <strong>of</strong> a Sea-Level Database for Irel<strong>and</strong>. Irish Journal <strong>of</strong> Earth Sciences 24, 13–27. Brooks, A. J., S. L. Bradley, R. J. Edwards, G. A. Milne, B. Horton, <strong>and</strong> I. Shennan. 2008. Postglacial relative sea-level observations from Irel<strong>and</strong> <strong>and</strong> their role in glacial rebound modelling. Journal <strong>of</strong> Quaternary Science 23, 175-192. Brown, A. G., G. Aalbersberg, M. Thorp, <strong>and</strong> P. Glanville. 2007. Alluvial Geoarchaeology in Irel<strong>and</strong>, in E. M. Murphy <strong>and</strong> N. J. Whitehouse (Eds). Environmental Archaeology in Irel<strong>and</strong>, pp. 241- 258. Oxford: Oxbow. Caseldine, C., G. Thompson, C. Langdon, <strong>and</strong> D. Hendon. 2005. Evidence for an extreme climatic event on Achill Isl<strong>and</strong>, Co. <strong>Mayo</strong>, Irel<strong>and</strong> around 5200–5100 cal. yr BP. Journal <strong>of</strong> Quaternary Science 20, 169–178. Caulfield, S., R. G. O’Donnell, <strong>and</strong> P. I. Mitchell. 1998. 14C Dating <strong>of</strong> a <strong>Neolithic</strong> Field System at Céide Fields, County <strong>Mayo</strong>, Irel<strong>and</strong>. Radiocarbon 40, 629-640. Gardiner, M. J., <strong>and</strong> T. Radford 1980. Soil Associations <strong>of</strong> Irel<strong>and</strong> <strong>and</strong> Their L<strong>and</strong> Use Potential: Explanatory Bulletin to Soil Map <strong>of</strong> Irel<strong>and</strong> 1980 Dublin: An Foras Talúntais. Greenwood, S. L., <strong>and</strong> C. D. Clark. 2009a. Reconstructing the last Irish Ice Sheet 1: changing flow geometries <strong>and</strong> ice flow dynamics deciphered from the glacial l<strong>and</strong>form record. Quaternary Science Reviews 28, 3085-3100. —. 2009b. Reconstructing the last Irish Ice Sheet 2: a geomorphologically-driven model <strong>of</strong> ice sheet growth, retreat <strong>and</strong> dynamics. Quaternary Science Reviews 28, 3101-3123. Hinch, J. d. W. 1913. The shelly drift <strong>of</strong> Glenulra <strong>and</strong> Belderrig, Co. <strong>Mayo</strong>. Irish Naturalist 22, 1-6. McCabe, A. M. 2008. Glacial Geology <strong>and</strong> Geomorphology: the L<strong>and</strong>scapes <strong>of</strong> Irel<strong>and</strong>. Edinburgh: Dunedin. McCabe, A. M., P. U. Clark, <strong>and</strong> J. Clark. 2005. AMS 14C dating <strong>of</strong> deglacial events in the Irish Sea Basin <strong>and</strong> other sectors <strong>of</strong> the British–Irish ice sheet. Quaternary Science Reviews 24, 1673- 1690. Sleeman, A. G. Editor. 1992. Geology <strong>of</strong> <strong>North</strong> <strong>Mayo</strong>: a geological description to accompany the bedrock geology 1:100,000 map series: Sheet 6, <strong>North</strong> <strong>Mayo</strong>. Dublin: Geological Survey <strong>of</strong> Irel<strong>and</strong>. Stone, J. J. 1991. <strong>North</strong> <strong>Mayo</strong> - Regional Geology, in P. Coxon (Eds). Fieldguide to the Quaternary <strong>of</strong> <strong>North</strong> <strong>Mayo</strong>, pp. 4 - 24. Dublin: Irish Association for Quaternary Studies. Symes, R. G., Traill, W.A, McHenry, A. 1881. Explanatory Memoir to Accompany Sheets 39, 40, 51, 52 <strong>and</strong> <strong>North</strong>ern Portion <strong>of</strong> 62 <strong>of</strong> the Maps <strong>of</strong> the Geological Survey <strong>of</strong> Irel<strong>and</strong>, including the country around Belmullet, Bangor, Corick, Belderg <strong>and</strong> Portacloy, <strong>and</strong> the Isl<strong>and</strong>s <strong>of</strong> Inishkea, Inishglora <strong>and</strong> Duvillaun. Dublin: HMSO. Turner, J. N., M. G. Macklin, A. F. Jones, <strong>and</strong> H. Lewis. 2010. New perspectives on Holocene flooding in Irel<strong>and</strong> using meta-analysis <strong>of</strong> fluvial radiocarbon dates. Catena 82, 183-190. 105
- Page 1 and 2:
Neolithic and Bronze Age Landscapes
- Page 3 and 4:
Table of Contents Introduction ....
- Page 5 and 6:
Scientific Research associated with
- Page 7 and 8:
Introduction This report reviews th
- Page 9 and 10:
- A summary of the radiocarbon dati
- Page 11 and 12:
Creating Digital Archaeological Lan
- Page 13 and 14:
Figure 2: Data Model for NBNM GIS R
- Page 15 and 16:
Figure 4: example of outputs at Cé
- Page 17 and 18:
Rathlackan As a result of a lack of
- Page 19 and 20:
Radiocarbon Dating A further tranch
- Page 21 and 22:
RATHLACKAN Lab Number F no S. No Co
- Page 23 and 24:
GLENULRA ENCLOSURE Notes Cal BC (95
- Page 25 and 26:
Lab Code Cutting Sample Material AR
- Page 27 and 28:
Charcoal analysis from Neolithic an
- Page 29 and 30:
Results Overall charcoal 83 samples
- Page 31 and 32:
Glenulra Scatter 92E140 Middle Neol
- Page 33 and 34:
Oak and birch were recorded from Cu
- Page 35 and 36:
35 30 no of samples 25 20 15 10 5 0
- Page 37 and 38:
Area A A long length of Neolithic f
- Page 39 and 40:
piece was 17 years old when cut, ba
- Page 41 and 42:
elating to midden B2P and from five
- Page 43 and 44:
1% 6% Corylus 1% 14% 25% 0% 2% 4% 4
- Page 45 and 46:
posts burnt in situ. Rather the pos
- Page 47 and 48:
When the charcoal is examined throu
- Page 49 and 50:
at Glenulra scatter. Alder was iden
- Page 51 and 52:
een freely available in the area. T
- Page 53 and 54:
References Byrne, G., Warren, G., W
- Page 55 and 56:
Verrill, L. and Tipping, R. 2010. U
- Page 57 and 58:
Table 3 Charcoal identifications fr
- Page 59 and 60: Sample Date Ctg Context Description
- Page 61 and 62: Sample Date Ctg Context Description
- Page 63 and 64: Sample Trench Time period Descripti
- Page 65 and 66: Sample Trench Time period Descripti
- Page 67 and 68: Sample Trench Time period Descripti
- Page 69 and 70: Sample Trench Time period Descripti
- Page 71 and 72: Sample Trench Time period Descripti
- Page 73 and 74: Sample Trench Time period Descripti
- Page 75 and 76: Sample Trench Time period Descripti
- Page 77 and 78: Sample Trench Time period Descripti
- Page 79 and 80: Table 7 Wood identification details
- Page 81 and 82: Table 8 Charcoal identifications fr
- Page 83 and 84: Cutting Sample Date Feature Descrip
- Page 85 and 86: Cutting Sample Date Feature Descrip
- Page 87 and 88: Cutting Sample Date Feature Descrip
- Page 89 and 90: Table 8 Sample assessment Rathlacka
- Page 91 and 92: Phase F. S. Trench Deposit type Loc
- Page 93 and 94: Behy-Glenulra: Céide Fields visito
- Page 95 and 96: A possible midden (B2P) contained a
- Page 97 and 98: Wild remains Hazelnut shell fragmen
- Page 99 and 100: References Beijerinck, W. 1947. Zad
- Page 101 and 102: Verrill, L. and Tipping, R. 2010. A
- Page 103 and 104: Soils and Geology Graeme Warren Thi
- Page 105 and 106: Figure 3: overview of geological fe
- Page 107 and 108: distinctive deposits and landscape
- Page 109: Figure 4: major landuse categories.
- Page 113 and 114: The first scientific paper on late
- Page 115 and 116: Also in the summer of 1963, fifty k
- Page 117 and 118: the earth for the bank coming from
- Page 119 and 120: dates from the macrofossil remains
- Page 121 and 122: New Research and Researchers Over t
- Page 123 and 124: Probed Surveys: Erris, Céide Field
- Page 125 and 126: Iron probes of varying lengths had
- Page 127 and 128: Céide hill twenty five years earli
- Page 129 and 130: Survey on the Glenamoy - Bartnatra
- Page 131 and 132: Bungurra River drains the Knocknalo
- Page 133 and 134: The elevation of the tombs, all sit
- Page 135 and 136: In 1936, 2 sub-rectangular cists, C
- Page 137 and 138: Dooncarton Southwest slope 3.15 km
- Page 139 and 140: The cross-section area occupied by
- Page 141 and 142: No upper boundary was located on Kn
- Page 143 and 144: The third house site, H3, on Gortme
- Page 145 and 146: The 2 court tombs, Ma38 and Ma23, l
- Page 147 and 148: This void is substantiated by exami
- Page 149 and 150: Survey from Ballinglen to Rathfran
- Page 151 and 152: Lissadrone basin. The peat cover is
- Page 153 and 154: Two similar large round cairns are
- Page 155 and 156: Wall Gaps Because of concealment an
- Page 157 and 158: supported by an orthostat visible u
- Page 159 and 160: and with different building techniq
- Page 161 and 162:
Survey Illustrations: Figure 1: Ove
- Page 163 and 164:
Figure 4: Seefin walls with associa
- Page 165 and 166:
Figure 7: Walls from the study area
- Page 167 and 168:
Figure 8: Cabintown Site A. 161
- Page 169 and 170:
Figure 11: Rathlackan sites H12 Fig
- Page 171 and 172:
Figure 15: Creevagh H5, Figure 16:
- Page 173:
Figure 19: Carrowkibbock Upper H20.